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handle: 10550/27905 , 10261/79755 , 1885/37039
The age of Neanderthal remains and associated sediments from El Sidrón cave has been obtained through different dating methods (14CAMS, U/TH, OSL, ESR and AAR) and samples (charcoal debris, bone, tooth dentine, stalagmitic flowstone, carbonate‐rich sediments, sedimentary quartz grains, tooth enamel and land snail shells). Detrital Th contamination rendered Th/U dating analyses of flowstone unreliable. Recent14C contamination produced spurious age‐values from charcoal samples as well as from inadequately pretreated tooth samples. Most consistent14C dates are grouped into two series: one between 35 and 40 ka and the other between 48 and 49 ka. Most ESR and AAR samples yielded concordant ages, ranging between 39 and 45 ka; OSL dating results permitted adequate bracketing of the sedimentary layer that contained the human remains. Our results emphasize the value of multi‐dating approaches for the establishment of reliable chronologies of human remains.
Stylommatophora 14C, dating method, geochronology, Asturias, Hominidae, Home de Neandertal, Aar, U/Th, thorium, Neanderthal, Pleistocene, uranium, Spain, Homo sapiens neanderthalensis, Geología, Dating, Keywords: carbon isotope, tooth, Osl, skeletal remains, Esr
Stylommatophora 14C, dating method, geochronology, Asturias, Hominidae, Home de Neandertal, Aar, U/Th, thorium, Neanderthal, Pleistocene, uranium, Spain, Homo sapiens neanderthalensis, Geología, Dating, Keywords: carbon isotope, tooth, Osl, skeletal remains, Esr
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